REPORT OF INVESTIGATIONS NO. 42 S Floridaon aquifer) A 1 832-154-1 3- 4 832-154-2'- (5Nonortesion pquifer) 3 mile Ronf ol at well 832-54-1,2 3 --------------- --- --- s soult h of Mascotte t-[.i 103 S i 102 101 100 99 o 813-149-2 (Non.oresan oquifer) 131 S4 ----------------- 813-149-1 ----- 128 - (Floridon aquifer) 27 2.5 miles north of Polk City _ .... r- I ^ I .~929 821-202-3 (Floridon aquifer in unconfined area) 9 9 rules east of Dode Cty Rtifoll at well 821-202-3 a: Q- .I 2 I JAN FEB MAR APR MAY JUNE JULY AUG SEPT OCT NOV DEC 1959 Figure 24. Hydrographs of water levels and rainfall at wells in the Green Swamp area, 1959. Water levels in most wells in the Green Swamp area show rises in response to local daily rainfalls. Only wells 810-136-2 and 815-139-3, located in the sandy ridges east of the Green Swamp area, show no response to local daily rainfall. Apparently, this is due to the high retention of the thick section of sand through which the water must percolate to reach the water table. Hydrographs of water levels in wells located in the central part of the Green Swamp area (figs. 27 and 28; wells 813-149-2, i 3 129-- -- -- - 813-150-2, 814-143-2, 822-149-2, 832-154-2) show that the water table declined less than 5 feet from a wet to a dry period (1959-62). near the surface and the aquifer afforded little capacity to store 21-5-,84132 2-4-,82142 hwta h ae talr elndls hn5fe rmawtt r eid(996) Durin th e er f15 n 90 h ae aleAine nEa